What is he best known for?
The fields of study he is best known for:
- Meteorology
- Mechanics
- Thermodynamics
Large eddy simulation, Meteorology, Planetary boundary layer, Turbulence and Mechanics are his primary areas of study.
His Large eddy simulation research incorporates elements of Cartesian coordinate system, Atmospheric sciences and Massively parallel.
His Roughness length study in the realm of Meteorology interacts with subjects such as Von Kármán constant.
Siegfried Raasch works in the field of Planetary boundary layer, focusing on Convective Boundary Layer in particular.
In his study, Turbulence kinetic energy is inextricably linked to Vortex, which falls within the broad field of Turbulence.
His work on Heat flux and Computer simulation is typically connected to Magnetosphere particle motion and Collision as part of general Mechanics study, connecting several disciplines of science.
His most cited work include:
- Improvement of the K-profile Model for the Planetary Boundary Layer based on Large Eddy Simulation Data (527 citations)
- An intercomparison of large-eddy simulations of the stable boundary layer (386 citations)
- PALM - A large-eddy simulation model performing on massively parallel computers (207 citations)
What are the main themes of his work throughout his whole career to date?
His main research concerns Large eddy simulation, Turbulence, Meteorology, Atmospheric sciences and Mechanics.
His work deals with themes such as Climatology, Mixed layer, Convection, Scalar and Turbulence kinetic energy, which intersect with Large eddy simulation.
His Turbulence study which covers Entrainment that intersects with Liquid water content.
His study in the field of Planetary boundary layer, Mesoscale meteorology and Latent heat is also linked to topics like Scintillometer.
His studies deal with areas such as Wind speed and Heat transfer as well as Planetary boundary layer.
His study in Mechanics is interdisciplinary in nature, drawing from both Settling and Classical mechanics.
He most often published in these fields:
- Large eddy simulation (41.87%)
- Turbulence (34.37%)
- Meteorology (31.87%)
What were the highlights of his more recent work (between 2017-2021)?
- Large eddy simulation (41.87%)
- Palm (5.00%)
- Turbulence (34.37%)
In recent papers he was focusing on the following fields of study:
His scientific interests lie mostly in Large eddy simulation, Palm, Turbulence, Urban climate and Microscale chemistry.
The concepts of his Large eddy simulation study are interwoven with issues in Sensible heat, Atmospheric sciences, Heat flux, Grid and Convective Boundary Layer.
Convective Boundary Layer is a subfield of Planetary boundary layer that Siegfried Raasch investigates.
His Turbulence study necessitates a more in-depth grasp of Mechanics.
Siegfried Raasch has researched Mechanics in several fields, including Coordinate system and Mesoscale meteorology.
His Meteorology research includes themes of Facade and Advection.
Between 2017 and 2021, his most popular works were:
- Overview of the PALM model system 6.0 (33 citations)
- A New Research Approach for Observing and Characterizing Land-Atmosphere Feedback (32 citations)
- Ventilation and Air Quality in City Blocks Using Large-Eddy Simulation—Urban Planning Perspective (31 citations)
In his most recent research, the most cited papers focused on:
- Meteorology
- Thermodynamics
- Mechanics
Siegfried Raasch mainly focuses on Large eddy simulation, Atmospheric sciences, Urban planning, Grid and Convective Boundary Layer.
His biological study spans a wide range of topics, including Sensible heat and Heat flux.
His Heat flux research incorporates themes from Monin–Obukhov similarity theory and Shear stress.
In his research on the topic of Urban planning, Inflow, City block, Atmospheric instability and Atmospheric model is strongly related with Air quality index.
His research in Grid intersects with topics in Mechanics, Intensity, Surface and Scalar.
Siegfried Raasch interconnects Convection, Turbulence kinetic energy and Altitude in the investigation of issues within Convective Boundary Layer.
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